August- September NSF NOAA NRL NCAR UW UM RAINEX Workshop, Miami, 5-7 June 2006
NSF NOAA NRL NCAR UW UM 5-7 June Workshop
Motivation for RAINEX Understanding Rapid Intensity Changes
Cat 2 Cat 3 Cat 5 Cat 4 Day Famous Rapidly Intensifing Storm Hurricane Opal (1995) Pressure drop How do interactions of eyewalls & rainbands in the mature storm… … lead to intensity changes like these? rainband Intensity change problem:
RAINEX Flight Coordination ELDORA radar
KatrinaOpheliaRita Hurricanes investigated in RAINEX
Katrina
Katrina-28 August NRL convective upwind stratiform downwind Atlas et al. ‘ 63
Katrina-28 August ELDORA data Ref Vel Barnes et al. ‘ 83 NRL
Katrina-28 August Confirms “ Barnes ” structure
Rita
RAINEX Flights in Hurricane Rita
0 ºC Rita- 21 September Intensifying to Cat. 5 EyeEyewall
Rita- 22 September-Concentric Eyewalls
Rita- 23 September-Sheared Shear Rogers et al. ‘ 03
Ophelia
A B Ophelia-9 September-Dry Midlevel Inflow B A Dry air Ref Vel
Data Availability
CONCLUSIONS RAINEX Notables: 3 hurricanes—Katrina, Ophelia, & Rita Innovative satellite-based flight control First use of ELDORA in a hurricane Data available via NCAR Field Catalog Katrina and Rita details: K & R’s spiral rainbands had Atlas & Barnes structures R sampled in 3 stages: rapid int., 2nd eyewall, shear Echo cores in eyewalls were linear & oblique Moat region had eye-like sounding Dry air entered in subsiding mesoscale midlevel inflows KatrinaOpheliaRita
How do rainbands form and evolve? How do rainbands contribute/influence the hurricane strength and evolution? Do the rainbands have any influence on the formation of secondary eyewall structure? If so, how? What is the influence/impact of secondary eyewall generation on the storm intensity? How do the concentric eyewall circulations influence overall storm intensity and structure? How does the convective "burst" affect initial storm growth? How do rainbands and eyewall organize in early stages of storm development? RAINEX Science Questions RAINEX Workshop, Miami, 5-7 June 2006